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The locations of National Register properties and districts (at least for all showing latitude and longitude coordinates below) may be seen in a map by clicking on "Map of all coordinates". [1] There are 4 properties and districts listed on the National Register in the county, including 1 National Historic Landmark
Recorded Texas Historic Landmark, now a Courtyard by Marriott hotel 14: Green Acres Apartments: March 21, 2024 : 3118 SW 15th Ave. Amarillo: 15: Herring Hotel: Herring Hotel: January 25, 2024 : 311 SE 3rd Avenue
Palo Duro Canyon is a canyon system of the Caprock Escarpment located in the Texas Panhandle near the cities of Amarillo and Canyon. [2] A large canyon system in the south-central United States , it is roughly 25–40 mi (40–64 km) long and has an average width of 6 mi (9.7 km), but reaches a width of 20 mi (32 km) at places.
It is a two-story construction, its oldest portion a log cabin which predates the American Civil War. The main portion of the house, built beginning in 1879, has rough stone walls on the ground floor and a wood-framed second story. Nearby outbuildings include the original 19th-century stables and corral, and a house for bunking ranch hands. [3]
The Pratt family spent summers at the cabin, which they called the Stone Cabin, and briefly lived there during Wallace Pratt's early retirement. An earlier experience being trapped at the Stone Cabin during a flood caused Pratt to reconsider its use as a full-time residence, so a second home, the Ship On The Desert , was constructed outside of ...
The canyon is now about 800 feet (240 meters) deep and about 20 miles (30 kilometers) across, making it the second largest canyon in the United States behind Arizona’s Grand Canyon. Comprised of sedimentary rock layers, the oldest exposed rocks in Palo Duro were deposited more than 250 million years ago, during the Permian Period.
The formation crops out along Palo Duro Canyon and the Canadian River and their tributaries. [1] It is also widespread in the Sangre de Cristo Mountains. [4] The formation is interpreted as deposition in a braided stream system. [5] The lower beds at Palo Duro Canyon contain unusual cone-shaped iron concretions that likely formed in the vadose ...
[2] [3] Overall, Tierra Blanca Creek descends 1,050 ft (320 m) from its headwaters in Eastern New Mexico to its confluence with Palo Duro Creek at the head of Palo Duro Canyon. The creek's water levels are variable, and it is not unusual for some parts of the creek to be reduced to a small trickle or dry completely during frequent periods of ...
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